Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Natalia I. Vetrova"'
Publikováno v:
Minerals, Vol 12, Iss 10, p 1282 (2022)
The Tannuola terrane, located in the northern Central Asian Orogenic Belt, comprises magmatic rocks, attributed to island-arc and collisional settings during the Early Cambrian to the Late Ordovician. However, zircon U-Pb age, geochemical, and Sr-Nd
Externí odkaz:
https://doaj.org/article/bcd74485042a4bd3a745db17d33320ff
Autor:
Evgeny V. Vetrov, Johan De Grave, Natalia I. Vetrova, Fedor I. Zhimulev, Simon Nachtergaele, Gerben Van Ranst, Polina I. Mikhailova
Publikováno v:
Minerals, Vol 11, Iss 6, p 604 (2021)
The West Siberian Basin (WSB) is one of the largest intracratonic Meso-Cenozoic basins in the world. Its evolution has been studied over the recent decades; however, some fundamental questions regarding the tectonic evolution of the WSB remain unreso
Externí odkaz:
https://doaj.org/article/306e5da0c91842cc812b865588072c41
Autor:
J. De Grave, S.V. Zhigalov, G.A. Babin, P.D. Kotler, N.N. Kruk, G.S. Fedoseev, Natalia I. Vetrova, E.V. Vetrov
Publikováno v:
Gondwana Research. 93:26-47
Late Paleozoic – early Mesozoic geological evolution of the Kolyvan-Tomsk Fold Zone (KTFZ) located in the northwestern part of the Central Asian Orogenic Belt is significant to understanding the tectonic transition from post-collision to intraplate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52820a8e457b07befeb4a12354151ada
https://doi.org/10.1016/j.gr.2021.01.008
https://doi.org/10.1016/j.gr.2021.01.008
Autor:
Johan De Grave, E.V. Vetrov, Natalia I. Vetrova, Gerben Van Ranst, Simon Nachtergaele, Polina I. Mikhailova, F.I. Zhimulev
Publikováno v:
Minerals
Volume 11
Issue 6
MINERALS
Minerals, Vol 11, Iss 604, p 604 (2021)
Volume 11
Issue 6
MINERALS
Minerals, Vol 11, Iss 604, p 604 (2021)
The West Siberian Basin (WSB) is one of the largest intracratonic Meso-Cenozoic basins in the world. Its evolution has been studied over the recent decades
however, some fundamental questions regarding the tectonic evolution of the WSB remain un
however, some fundamental questions regarding the tectonic evolution of the WSB remain un
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2479da36a7ec48329305124ed477fa76
https://doi.org/10.3390/min11060604
https://doi.org/10.3390/min11060604
Publikováno v:
Gondwana Research. 51:255-271
This study provides 87 Sr/ 86 Sr, δ 13 C and δ 18 O data from the best-preserved limestone and dolomite of the Ediacaran carbonate-dominated Khorbusuonka Group of the Olenek Uplift, NE Siberian Craton, as well as detrital zircon geochronological da
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::75731005d46c741d6a549ea823b5e119
https://doi.org/10.1016/j.gr.2017.07.010
https://doi.org/10.1016/j.gr.2017.07.010
Autor:
Polina I. Mikhailova, Gerben Van Ranst, Johan De Grave, F.I. Zhimulev, Natalia I. Vetrova, E.V. Vetrov, Simon Nachtergaele
Publikováno v:
Minerals
Volume 10
Issue 1
MINERALS
Minerals, Vol 10, Iss 1, p 56 (2020)
Volume 10
Issue 1
MINERALS
Minerals, Vol 10, Iss 1, p 56 (2020)
In this study, we present zircon U/Pb, plagioclase and K-feldspar 40Ar/39Ar and apatite fission track (AFT) data along the South Tannuol Fault Zone (STFZ). Integrating geochronology and multi-method thermochronology places constraints on the formatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::29a544ed13e3e98a2e31320fa8654270
https://doi.org/10.3390/min10010056
https://doi.org/10.3390/min10010056